THE ROLES OF BOUNDARY-LAYER DYNAMICS ON THE DEVELOPMENT OF MADDEN-JULIAN OSCILLATION          下载免费PDF全文

巢纪平  林永辉  王斌 《Acta Meteorologica Sinica》1995,(2)

In this paper,a tropical atmospheric model of relevance to shorts-term climate variations(Wang and Li 1993)is util-ized for study of the development of Madden-Julian oscillation.The model contains an interactive process ofboundary-layer Ekman convergence and precipitation heating.The model is solved by expanding dependent variables interms of parabolic cylindrical functions in the meridional direction and truncating three meridional modes n=0,2,4 forequatorial symmetric solutions.The free wave solutions obtained under long-wave approximation are induced as aKelvin wave and two Rossby waves.After considering the effect of boundary-layer dynamic process,the modifiedKelvin wave becomes unstable in long-wave bands with a typical growth rate on an order of 10~(-6) s~(-1)and an eastwardphase speed of 10 m s~(-1);the most unstable mode is wavenumber one.These theoretical results are consistent with the ob-served Madden-Julian oscillation in equatorial area.For the two modified Rossby waves,one with a smaller meridionalscale(n=4)decays except for extra long-waves;the other with a larger meridional scale(n=2)grows in short-wavebands.This may be relevant to explaining the westward propagation of super cloud clusters in the Madden-Julianoscillation.The theory suggests that the boundary-layer dynamic process is an important mechanism in the develop-ment of the Madden-Julian oscillation.  相似文献   

A CASE OF MESOSCALE CONVECTIVE COMPLEX EVOLVING INTO A VORTEX   总被引：1，自引：0，他引：1       下载免费PDF全文

陶祖钰  王洪庆  白洁  朱文琴  石定朴  杨红梅 《Acta Meteorologica Sinica》1995,(2)

A case of mesoscale convective complex(MCC)which evolved into a vortex is documented in this paper.As theMCC entered into the dissipating phase,a well-defined spirally banded structure became visible in the satellite image.The blackbody temperature(TBB)of the residual cold-cloud-shield indicates the vortex existed in the layer from 400 to250 hPa.According to the upper air analysis,the upper level vortex was an anticyclone.The MCC-generated vortex wasvisualized in the satellite images because it was located in the subtropical high where the wind field was very weak.  相似文献   

辽西中生代花岗岩中锆石的地球化学演化特征及其地质意义     

刘成龙 《岩石矿物学杂志》1987,6(4):338-344

文中论述了辽西中生代花岗岩中锆石富∑REE、Mo,低Zr/Hf的成分特点。随岩浆演化,岩体由早侵入期次到晚侵入期次,锆石的Hf、∑REE、Th、U含量递增,Zr/Hf递减的演化规律明显。晚世代锆石较早世代更富含成矿元素(Mo)、稀土、放射性元素。指出锆石中成矿元素Mo的浓集,并伴随着Hf、∑REE、Th、U元素含量的相对增高,可作为岩体潜在成矿(Mo)的一种重要标志。锆石的矿物地球化学特征为区内花岗岩成因类型的划分提供了依据。  相似文献   

Laihunite—A new iron silicate mineral     

Laihunite Research Group 《中国地球化学学报》1982,1(1):105-114

Laihuite reported in the present paper is a new iron silicate mineral found in China with the following characteristics:

1. This mineral occurs in a metamorphic iron deposit, associated with fayalite, hypersthene, quartz, magnetitc, etc.
2. The mineral is opaque, black in colour, thickly tabular in shape with luster metallic to sub-metallic, two perfect cleavages and specific gravity of 3.92.
3. Its main chemical components are Fe and Si with Fe³⁺>Fe²⁺. The analysis gave the formula of Fe Fe _1.00 ³⁺ ·Fe _0.58 ²⁺ ·Mg _0.03 ²⁺ ·Si_0.96O₄.
4. Its DTA curve shows an exothermic peak at 713°C.
5. The mineral has its own infrared spectrum distinctive from that of other minerals.
6. This mineral is of orthorhombic system; space group:C _2h ^/5 ?P2₁/c; unit cell:α=5.813ű0.005,b=4.812ű0.005,c=10.211ű0.005,β=90.87°.
7. The Mössbauer spectrum of this mineral is given, too.

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Discovery of A-type Granite Zone and Its Geodynamic Significance in the Western Kunlun Mts., China     

JIANG Yao-hui  YANG Wanzhi State Key Laboratory for Mineral Deposits Research  Department of Earth Sciences  Nanjing University  Nanjing    Nanjing Institute of Geology  Mineral Resources  Ministry of Land  Resource. Nanjing    Xinjian 《Continental Dynamics》2001,(2)

l. IntroductionGranite distributes widely in western KunlunMts. Many researches have been conducted byscientists (Wang Yuzhen et.al., l987; Zhang Yuquanet.al., l989, Fang Xilian et.al., I990, Jiang Chunfaet.al., 1992; Pan Yusheng, l992, Xu Ronghua et.al.,l 994; Jing Daogui et.al., l996, Zhang Yuquan et.al.,l998). But all of the researches have been donealong Sino-Pakistan road and Xinjiang-Tibet roadt"ith fOcus on isotopic dating of the intrusion andconducted a few on origin and tect…  相似文献   

生态屏障约束下的综合功能区划研究——以云南省昭通市为例(英文)     

杜瑜  王传胜  赵海英  杨晓光 《地理学报(英文版)》2007,(3)

Ecological shelter zones reconstruction is an ecosystem restoration and conserva-tion project aimed to the ecological safety of nations,regions and basins. Reconstruction of ecological shelter zones of the upper reaches of the Yangtze River became one of the most important tasks of Western Development strategy. This article,taking Zhaotong as an exam-ple,studies the functional regionalization of ecological shelter zones. The study supplies a case for functional regionalization of small and medium regions whose main tasks are envi-ronment reservation. With the guidance of theories of functional regionalization,and based on the analysis of Zhaotong's natural,ecological and socioeconomic factors,the paper suggests five principles for factors selection. These principles include: (1) reversing order evaluation; (2) selecting main factors; (3) keeping the integrality of administrative regions of towns; and (4) making the products acceptable by local government. To analyze spatial status of selected factors,LUCC data in 2002,1:50,000 relief maps and town-unit socioeconomic statistical data in 2004 are used. RS and GIS tools are also applied to melt traditional and modern geo-graphical methods. This would be useful to functional regionalization research in mountain-ous areas. As a conclusion,the leading functional regions of ecological conservation or economic development are suggested,respectively. Zhaotong city is divided into two-level functional regions. The first-level includes three leading functional regions and they will lead developing direction of sub-regions. The second-level includes eight sub-regions,which are policy implemented regions,and will supply guidance to Zhaotong's ecological shelter zones reconstruction.  相似文献   

中国含油气盆地构造分析主要进展与展望   总被引：4，自引：2，他引：4  

汤良杰  金之钧等 《地质论评》2002,48(2):182-192

本文简要总结了中国含油气盆地构造分析的主要进展。中国区域大地构造理论特别是板块构造理论，对于指导盆地构造研究起了重要作用。通过各种地球物理探测方法，揭示了中国含油气盆地的上地幔结构，地壳结构、基底结构与盖层构造的关系。中国含油气盆地在地质历史中的演化过程十分复杂，伸展盆地、前陆盆地、走滑盆地、克拉通盆地和叠合具有各自独特的地球动力学系统。构造样式分析是盆地构造分析的重要方面，直接与寻找油气圈闭有关，可以划分出伸展构造、挤压构造、走滑构造、反转构造和潜山－披覆构造等。断裂和不含油气盆地中的重要构造要素，控制着油气运聚成藏、叠合盆地多期成盆、多期改造造成的复杂构成图像，是中国含油气盆地的重要特色之一。展望21世纪 中国油气盆地构造分析，需要重点关注的是：叠合盆地形成演化和地球动力学过程分析；盆－山耦合过程的深部－浅部耦全过程分析；盆地三维构造精细描述和盆地模拟技术，盐构造和天然气构造分析。  相似文献   

一种基于GIS的矿产资源潜力评价的自动制图模型     

陈永良  刘大有 《地质论评》2002,48(3):324-329

在基于GIS技术的矿产资源评价工作中,矿产资源潜力评价的自动制图模型通常用来统计综合多源地学信息以便自动圈定成矿远景靶区。在本文中,笔者以人工智能研究领域中的一种不确定推理模型——确定性理论为基础,提出了一种新的矿产资源潜力评价的自动制图模型——合成有矿可信度模型。该模型可以根据研究区各种成矿有利和不利证据的空间分布图,统计生成对应于每一种证据的有矿可信度栅格图,然后,按照特定的有矿可信度合成规则,将所有的有矿可信度栅格图统计综合生成合成有矿可信度栅格图。以该图为依据,可以把研究区内合成有矿可信度相对较高的成矿远景区圈定出来。也可以生成研究区合成有矿可信度等值线图。应用该模型预测了新疆北部多拉纳萨依—阿舍勒地区的多金属成矿远景,并将预测结果与证据加权模型预测结果进行了比较,两种模型的预测结果基本相似,证明了该模型的有效性和实用性。  相似文献   

断裂构造研究进展对工程地质学的启示   总被引：4，自引：0，他引：4  

陈昌彦  张李节等 《地质论评》2002,48(5):487-494

在长期地质作用下形成的岩体和岩体结构是工程地质学研究的基本内容，它们的形成和演化主要受控于构造作用，而系统地解析体所经历的构造作用是认知岩体结构，抽象和概括岩体工程地质模型的突破口，因此，重视和应用现代构造地质学研究的新理论，新方法必将会对岩体工程地质学研究起着重要的指导意义。本文系统总结了与工程地质研究相关的现代构造地质学理论和思维观的研究进展，在此基础上分析了这些理论方法对工程地质工作的启示和指导意义，希望起到抛砖引玉的作用。  相似文献   

Hydrothermal Alteration Zoning and Kinetic Process of Mineral-Water Interactions     

ZHANG Ronghu  HU Shumin  SU YanfengOpen Research Laboratory of Geochemical Kinetics  Institute of Mineral Resources  Chinese Academy of Geological Sciences  Baiwanzhuang Ro  Beijing  China 《《地质学报》英文版》2002,76(3):351-366

This study reports the kinetic experimental results of albite in water and in KCI solution at 22 MPa in the temperature range of 25 to 400℃. Kinetic experiments have been carried out in an open flow-through reaction system (packed bed reactor). Albite dissolution is always incongruent in water at most temperatures, but becomes congruent at 300℃ (close to the critical point 374℃). At temperatures from 25 to 300℃, the incongruent dissolution of albite is reflected by the fact that sodium and aluminum are easily dissolved into water; from 300 to 400℃ it is reflected by silicon being more easily dissolved in water than Al and Na. Maximum albite dissolution rates in the flow hydrothermal systems have been repeatedly observed at 300℃, independent of flow rates.The kinetic experiments of albite dissolution in a KCl aqueous solution (0.1 mol KCl) indicate that the dissolution rate of albite increases with increasing temperature. Maximum silicon release rates of albite have been observed at 400℃, while ma  相似文献